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Date Published: 12/06/2013
Online Published: 12/06/2013
Abstract Views: 19
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DOI: https://doi.org/10.52714/dthu.3.6.2013.40
Issue
No. 3 (2013): Part B - Natural Sciences
Section
Natural Sciences Issue
How to Cite
Dang, T. H. (2013). Ảnh hưởng của các hồ chứa trên lưu vực sông Hồng đến quá trình chuyển tải phù sa của sông: ví dụ tại Trạm thủy văn Hà Nội. Dong Thap University Journal of Science, 3, 76-83. https://doi.org/10.52714/dthu.3.6.2013.40

Ảnh hưởng của các hồ chứa trên lưu vực sông Hồng đến quá trình chuyển tải phù sa của sông: ví dụ tại Trạm thủy văn Hà Nội

Thi Ha Dang1
1 Ba Ria - Vung Tau University

Main Article Content

Abstract

This study is based on the data of the Red River's annual discharge and sediment transport between 1960 and 2010, documented at the Hanoi gauging station. The results showed that on a regular basis the annual discharge and sediment transport varied from 2665m3/s to 5058m3/s and 12×106 t/yr to 201×106 t/yr, respectively. Although the sediment transport is strongly related to the hydrological conditions, it has significantly decreased since the reservoirs came into operation. Specifically, since 1989 (the year of Hoa Binh reservoir in operation), the sediment transport decreased from 120×106 t/yr to 58×106 t/yr and since Tuyen Quang and Dai Thi reservoirs were in operation (2007), the transport volume was down to 19.7×106 t/yr. This indicates a strong impact of the reservoirs on the natural sediment formation of the Red River, causing erosion in the coastal area and ecological imbalance on the Red River delta.

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References

[1]. Dai S.B., Yang S.L. và Li M. (2009). “The sharp decrease in suspended sediment supply from China’s rivers to the sea: anthropogenic and natural causes”. Hydrological Sciences Journal (54), 135-146.
[2]. Dang T.H., Coynel A., Orange D., Blanc G., Etcheber H. và Le L.A. (2011) “Long-term monitoring (1960-2008) of the river- sediment transport in the Red River Watershed (Vietnam): temporal variability and dam impact”. Science of the Total Environment (số 408), tr. 4646-4664.
[3]. Dang T.H. (2011). Erosion and tranferts de metieres en suspension, carbone et metaux dans le bassin versant du Fleuve Rouge depuis la frontiere sino-vietnamienne jusqu’a l’entree du delta. Luận án Tiến sỹ, Đại học Bordeaux 1, Pháp.
[4]. Kao S.J. và Liu K.K (1996). “Particulate organic carbon export from a subtropical mountainous river (Lanyang His) in Taiwan”. Limnology and Oceanography (số 41), tr. 1749-1757.
[5]. Milliman J.D. và Syvitski J.P.M. (1992). “Geomorphic/Tectonic control of sediment discharge to the Ocean: The importance of small mountainous river”. The Journal of Geology (số 100), tr. 525-544.
[6]. Milliman J.D., Farnsworth K.L., Jones P.D., Xu K.H. và Smith L.C. (2008). “Climatic and anthropogenic factors affecting river discharge to the global ocean, 1951-2000”. Global and Planetary Change (số 62), tr.187-194.
[7]. Milliman J.D. và Meade R.H. (1983). “World-wide delivery of river sediment to the oceans”. The journal of Geology (số 91), tr. 1-21.
[8]. Lu X. và Jiang T. (2009). “Larger Asian rivers: Climate change, river flow and sediment flux”. Quaternary International (số 208), tr. 1-3.
[9]. Schafer J., Blanc G., Maillet N, Maneux E., Etcheber H. (2002). “Ten years observation of the Gironde tributary fluvial system : fluxes of suspended matter, particulates organic carbon and cadmium”. Marine Chemistry (số 79), tr. 229-242.